Magnetic scanning and interpretation of paleomagnetic data from Prague Synform?s volcanics

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F13%3A00389165" target="_blank" >RIV/67985831:_____/13:00389165 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11310/13:10133016

Výsledek na webu

<a href="http://dx.doi.org/10.1007/s11200-012-0723-4" target="_blank" >http://dx.doi.org/10.1007/s11200-012-0723-4</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s11200-012-0723-4" target="_blank" >10.1007/s11200-012-0723-4</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Magnetic scanning and interpretation of paleomagnetic data from Prague Synform?s volcanics

Popis výsledku v původním jazyce

Magnetic images have been produced at the distance of 0.1 mm from the polished basaltic thin sections of rocks from Prague Synform in Barrandian area. Three different magnetic textures were seen and when combined with optical imaging could be related topetrological features. The first magnetic texture revealed that most of the magnetic signature is localized within the amygdales formed later after the basalts became part of the sedimentary sequence. The second texture showed that the basaltic body contains large grain size distribution of magnetic carriers possibly with variable viscous magnetizations. The third texture suggested a presence of magnetic anisotropy of igneous origin. Such textural magnetic information along with the paleomagnetic characteristics of the basaltic rocks of Silurian age constrained the overall geological interpretation.

Název v anglickém jazyce

Magnetic scanning and interpretation of paleomagnetic data from Prague Synform?s volcanics

Popis výsledku anglicky

Magnetic images have been produced at the distance of 0.1 mm from the polished basaltic thin sections of rocks from Prague Synform in Barrandian area. Three different magnetic textures were seen and when combined with optical imaging could be related topetrological features. The first magnetic texture revealed that most of the magnetic signature is localized within the amygdales formed later after the basalts became part of the sedimentary sequence. The second texture showed that the basaltic body contains large grain size distribution of magnetic carriers possibly with variable viscous magnetizations. The third texture suggested a presence of magnetic anisotropy of igneous origin. Such textural magnetic information along with the paleomagnetic characteristics of the basaltic rocks of Silurian age constrained the overall geological interpretation.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

<a href="/cs/project/GAP210%2F10%2F2351" target="_blank" >GAP210/10/2351: Paleomagnetismus a geochemie vulkanických hornin: Implikace pro paleopozici a vývoj pražské pánve (sv. ordovik - sp. devon)</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Studia geophysica et geodaetica

ISSN

0039-3169

e-ISSN

—

Svazek periodika

57

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

15

Strana od-do

103-117

Kód UT WoS článku

000314301200007

EID výsledku v databázi Scopus

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